In addition, the (CIW)14 layer is thicker in September 1997. This indicates that the

volume of (CIW)14 has increased. This decrease of temperature and increase in thickness can be explained only if there is advection of cold water with the upper layer from the strait. Since the lower layer is colder in the spring months, the (CIW)14 thickness (9–70 m) covers the lower layer at station K0 in May 1997. In 1998, (CIW)14 is observed from May to September at station K2, from May to August at stations K0, B13 and M8, and from June to August at stations B7 and B2. Rapamycin datasheet In July 1998, the upper layer is colder along the strait so that the temperature of the surface layer at station B2 is less than 13.0 °C (Figure 6). For this reason, the (CIW)14 layer starts at 1 m depth at station B2 (Table 1). On the other hand, at station M8, the (CIW)14 layer is thicker in this month. Monthly fluctuations of the thickness of (CIW)14 at station M8 indicate the entrance of cold water to the Sea of Marmara through the strait. In September, (CIW)14 is very thin at station K2 and does not enter the strait. In 1999, cold water (CIW)14 is

observed in the Black Sea exit of the strait (station K2) and in the Sea of Marmara (at station M8) from June to October. At station K2, excluding ITF2357 solubility dmso the upper 7 m, the temperature of the entire water column is less than 14 °C in May 1999. The upper limit of the (CIW)14 is found at 38 m depth in July at station K2 owing to Danubian-influenced water, as mentioned before (Figure 2). The thickness of (CIW)14 increases in August 1999 at station K2. In September, the amount of (CIW)14 decreases at station K2 and it does not enter the strait. On the other hand, in October 1999, the amount of (CIW)14 increases compared to September and its minimum temperature is ∼ 7.9 °C compared to 11.6 °C in September. This increase is thought to be due to the advection of CIW to the area by the Rim Current. In 2000, CHIR-99021 clinical trial the thickness of (CIW)14 decreases in both exits of the strait. In the Black Sea exit of the strait, (CIW)14 is not observed after July, and consequently, it is

not observed at station M8 either. Examination of (CIW)14 indicates that the cold water existing in the Black Sea exit of the strait influences the cold water in the Sea of Marmara. The annual and monthly fluctuations in the amount of (CIW)14 have similar characteristics in the Black Sea and the Sea of Marmara. This similarity leads to the consideration that the cold layer in the Sea of Marmara is mostly supported by the cold layer in the Black Sea. Seasonal and spatial variations of (CIW)14 (modified CIW) in the two exit regions of the Strait of Istanbul are studied. (CIW)14 is usually observed from May to September in the Black Sea exit of the strait. In some years it is also observed in October or November.